Hostname: page-component-76fb5796d-zzh7m Total loading time: 0 Render date: 2024-04-26T09:40:54.277Z Has data issue: false hasContentIssue false
  • English
  • Français

Characteristics of heavy minerals and grain size of surface sediments on the continental shelf of Prydz Bay: implications for sediment provenance

Published online by Cambridge University Press:  24 November 2015

Haozhuang Wang ,
Zhihua Chen ,
Kunshan Wang ,
Helin Liu ,
Zheng Tang  and
Yuanhui Huang
Haozhuang Wang
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
Zhihua Chen*
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
Kunshan Wang
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
Helin Liu
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
Zheng Tang
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
Yuanhui Huang
Affiliation:
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China Key Laboratory of Marine Sedimentology & Environmental Geology, State Oceanic Administration, Qingdao 266061, China
*
*corresponding author:chenzia@fio.org.cn
Get access Rights & Permissions [Opens in a new window]

Abstract

Data on grain size and heavy mineral composition for surface sediments on the Prydz Bay continental shelf was analysed to identify sediment features and provenance. The grain size composition of surface sediments indicate spatial variations in the glaciomarine environment and the key factors influencing sedimentation, which on the shelf include topography/water depth, currents and icebergs. The study area was divided into two sections by Q-type factor analysis: section I included Prydz Channel, Amery Basin and Svenner Channel, and section II included Four Ladies Bank, Fram Bank and the area in front of the Amery Ice Shelf. Sedimentation in section I is mainly controlled by currents and topography/water depth. However, in section II, icebergs/floating ice masses, the Amery Ice Shelf and currents have prominent effects on sedimentation. The heavy mineral composition indicates that surface sediments on the eastern side of the bay, including Four Ladies Bank, are primarily derived from Princess Elizabeth Land. Sediments in the area in front of the Amery Ice Shelf, Svenner Channel, Amery Basin and Prydz Channel have a mixed source from the eastern regions around the bay, including the Prince Charles Mountains and Princess Elizabeth Land. The contribution from Mac. Robertson Land to sediment at Fram Bank is limited.

Keywords

grain sizeheavy mineralsPrydz Baysediment provenancesurface sediment
Type
Earth Sciences
Information
Antarctic Science , Volume 28 , Issue 2 , April 2016 , pp. 103 - 114
Check for updates
Copyright
© Antarctic Science Ltd 2015 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Allison, I. 1989. Pack-ice drift off East Antarctica and some implications. Annals of Glaciology, 12, 1–8.Google Scholar
Berg, S., Wagner, B., Cremer, H., Leng, M.J. & Melles, M. 2010. Late Quaternary environmental and climate history of Rauer Group, East Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 297, 201–213.CrossRefGoogle Scholar
Boger, S.D., Wilson, C.J.L. & Fanning, C.M. 2001. Early Paleozoic tectonism within the East Antarctic craton: the final suture between east and west Gondwana? Geology, 29, 463–466.2.0.CO;2>CrossRefGoogle Scholar
Borchers, A., Voigt, I., Kuhn, G. & Diekmann, B. 2011. Mineralogy of glaciomarine sediments from the Prydz Bay–Kerguelen region: relation to modern depositional environments. Antarctic Science, 23, 164–179.CrossRefGoogle Scholar
Crespin, J., Yam, R., Crosta, X., Massé, G., Schmidt, S., Campagne, P. & Shemesh, A. 2014. Holocene glacial discharge fluctuations and recent instability in East Antarctica. Earth and Planetary Science Letters, 394, 38–47.CrossRefGoogle Scholar
Diekmann, B. 2007. Sedimentary patterns in the late Quaternary Southern Ocean. Deep Sea Research II - Topical Studies in Oceanography, 54, 2350–2366.CrossRefGoogle Scholar
Diekmann, B. & Kuhn, G. 1999. Provenance and dispersal of glacial–marine surface sediments in the Weddell Sea and adjoining areas, Antarctica: ice-rafting versus current transport. Marine Geology, 158, 209–231.CrossRefGoogle Scholar
Dirks, P.H.G.M. & Wilson, C.J.L. 1995. Crustal evolution of the East Antarctic mobile belt in Prydz Bay: continental collision at 500 Ma? Precambrian Research, 75, 189–207.CrossRefGoogle Scholar
Dou, G. 1999. Incipient motion of coarse and fine sediment. Journal of Sediment Research, 6, 1–9. [Chinese].Google Scholar
Ehrmann, W. & Polozek, K. 1999. The heavy mineral record in the Pliocene to Quaternary sediments of the CIROS-2 drill core, McMurdo Sound, Antarctica. Sedimentary Geology, 128, 223–244.CrossRefGoogle Scholar
Ergin, M., Keskin, Ş., Doğan, A.U., Kadioğlu, Y.K. & Karakaş, Z. 2007. Grain size and heavy mineral distribution as related to hinterland and environmental conditions for modern beach sediments from the Gulfs of Antalya and Finike, eastern Mediterranean. Marine Geology, 240, 185–196.CrossRefGoogle Scholar
Fitzsimons, I.C.W. & Harley, S.L. 1991. Geological relationships in high‐grade gneiss of the Brattstrand Bluffs coastline, Prydz Bay, East Antarctica. Australian Journal of Earth Sciences, 38, 497–519.CrossRefGoogle Scholar
Forsberg, C.F., Florindo, F., Grützner, J., Venuti, A. & Solheim, A. 2008. Sedimentation and aspects of glacial dynamics from physical properties, mineralogy and magnetic properties at ODP Sites 1166 and 1167, Prydz Bay, Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 260, 184–201.CrossRefGoogle Scholar
Fricker, H.A., Warner, R.C. & Allison, I. 2000. Mass balance of the Lambert Glacier-Amery Ice Shelf system, East Antarctica: a comparison of computed balance fluxes and measured fluxes. Journal of Glaciology, 46, 561–570.CrossRefGoogle Scholar
Gao, S. & Collins, M. 2001. The use of grain size trends in marine sediment dynamics: a review. Chinese Journal of Oceanology and Limnology, 19, 265–271.Google Scholar
Harris, P.T. & O’Brien, P.E. 1998. Bottom currents, sedimentation and ice-sheet retreat facies successions on the Mac Robertson shelf, East Antarctica. Marine Geology, 151, 47–72.CrossRefGoogle Scholar
Harris, P.T., Taylor, F., Pushina, Z., Leitchenkov, G., O’Brien, P.E. & Smirnov, V. 1998. Lithofacies distribution in relation to the geomorphic provinces of Prydz Bay, East Antarctica. Antarctic Science, 10, 227–235.CrossRefGoogle Scholar
Hauptvogel, D.W. & Passchier, S. 2012. Early–Middle Miocene (17–14 Ma) Antarctic ice dynamics reconstructed from the heavy mineral provenance in the AND-2A drill core, Ross Sea, Antarctica. Global and Planetary Change, 82, 38–50.CrossRefGoogle Scholar
Hodgkinson, R.P., Colman, R.S., Kerry, K.P. & Robb, M. 1988. Water currents in Prydz Bay, Antarctica during 1985. ANARE Research Notes, No. 59, 127 pp.Google Scholar
Hodgkinson, R.P., Colman, R.S., Robb, M. & William, R. 1991a. Current meter moorings in the region of Prydz Bay, Antarctica, 1986. ANARE Research Notes, No. 81, 130 pp.Google Scholar
Hodgkinson, R.P., Colman, R.S., Robb, M. & Williams, R. 1991b. Current meter moorings in the region of Prydz Bay, Antarctica, 1987. ANARE Research Notes, No. 82, 68 pp.Google Scholar
Hodgson, D.A., Nood, P.E., Vyverman, W., Bryant, C.L., Gore, D.B., Appleby, P., Gilmour, M., Verleyen, E., Sabbe, A., Jones, V.J., Ellis–Evans, J.C. & Wood, P.B. 2001. Were the Larsemann Hills ice-free through the Last Glacial Maximum? Antarctic Science, 13, 440–454.CrossRefGoogle Scholar
Li, F., Ginoux, P. & Ramaswamy, V. 2008. Distribution, transport, and deposition of mineral dust in the Southern Ocean and Antarctica: contribution of major sources. Journal of Geophysical Research - Atmospheres, 113, 10.1029/2007JD009190.Google Scholar
Li, M. 2006. Geochronology and geochemistry of granitoids from the Prydz Belt, East Antarctica, and their tectonic implications. PhD thesis, Chinese Academy of Geological Sciences, 73 pp. [Unpublished].Google Scholar
Lilly, K., Fink, D., Fabel, D. & Lambeck, K. 2010. Pleistocene dynamics of the interior East Antarctic Ice Sheet. Geology, 38, 703–706.CrossRefGoogle Scholar
Liu, X.C., Jahn, B.-M., Zhao, Y., Li, M., Li, H.M. & Liu, X.H. 2006. Late Pan-African granitoids from the Grove Mountains, East Antarctica: age, origin and tectonic implications. Precambrian Research, 145, 131–154.CrossRefGoogle Scholar
MacKintosh, A.N., Verleyen, E., O’Brien, P.E., White, D.A., Jones, R.S., McKay, R., Dunbar, R., Gore, D.B., Fink, D., Post, A.L., Miura, H., Leventer, A., Goodwin, I., Hodgson, D.A., Lilly, K., Crosta, X., Golledge, N.R., Wagner, B., Berg, S., van Ommen, T., Zwartz, D., Roberts, S.J., Vyverman, W. & Masse, G. 2014. Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum. Quaternary Science Reviews, 100, 10–30.CrossRefGoogle Scholar
O’Brien, P.E. & Harris, P.T. 1996. Patterns of glacial erosion and deposition in Prydz Bay and the past behaviour of the Lambert Glacier. Papers and proceedings of the Royal Society of Tasmania, 130, 79–85.CrossRefGoogle Scholar
O’Brien, P.E. & Leitchenkov, G. 1997. Deglaciation of Prydz Bay, East Antarctica, based on echo sounding and topographic features. Antarctic Research Series, 71, 109–126.Google Scholar
Passchier, S., O’Brien, P.E., Damuth, J.E., Januszczak, N., Handwerger, D.A. & Whitehead, J.M. 2003. Pliocene–Pleistocene glaciomarine sedimentation in eastern Prydz Bay and development of the Prydz trough-mouth fan, ODP Sites 1166 and 1167, East Antarctica. Marine Geology, 199, 279–305.CrossRefGoogle Scholar
Smith, N.R., Dong, Z.Q., Kerry, K.R. & Wright, S. 1984. Water masses and circulation in the region of Prydz Bay, Antarctica. Deep-Sea Research I - Oceanographic Research Papers, 31, 1121–1147.CrossRefGoogle Scholar
Tingey, R.J. 1991. The geology of Antarctica. Oxford: Oxford University Press, 680 pp.Google Scholar
Vaz, R.A.N. & Lennon, G.W. 1996. Physical oceanography of the Prydz Bay region of Antarctic waters. Deep-Sea Research I - Oceanographic Research Papers, 43, 603–641.Google Scholar
White, D.A., Bennike, O., Berg, S., Harley, S.L., Fink, D., Kiernan, K., McConnell, A. & Wagner, B. 2009. Geomorphology and glacial history of Rauer Group, East Antarctica. Quaternary Research, 72, 80–90.CrossRefGoogle Scholar
Wilson, T., Grunow, A.M. & Hanson, R.E. 1997. Gondwana assembly: the view from southern Africa and East Gondwana. Journal of Geodynamics, 23, 263–286.CrossRefGoogle Scholar
Wu, C.D., Lin, C.S., Shen, Y.P. & Feng, X. 2005. Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China. Progress in Natural Science, 15, 633–640.Google Scholar
Zhao, J.X., Ellis, D.J., Kilpatrick, J.A. & McCulloch, M.T. 1997. Geochemical and Sr-Nd isotopic study of charnockites and related rocks in the northern Prince Charles Mountains, east Antarctica: implications for charnockite petrogenesis and Proterozoic crustal evolution. Precambrian Research, 81, 37–66.CrossRefGoogle Scholar